Normal Fault Cross Section Diagram. Extend and thin crust. This movement is the opposite or reverse to that seen in normal faults which is the reason why they are called reverse dip slip faults reverse faults.
Low angle normal fault footwall gneiss hanging wall shallow. A elevated right over left. As this happens the crust is lengthened stretched apart and thinned figure 829.
What type of fault is it.
Separation faults in wells fault propagation terminology hanging wall foot wall. View the full answer. As this happens the crust is lengthened stretched apart and thinned figure 829. One fault block moves upward compared to the other figure 3.